Archeometriai Műhely 2007/2., Supplement for Gherdán et al. 1
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1 Archeometriai Műhely 2007/2., Supplement for Gherdán et al. 1 xx2a 1 N light brown + N yellowish brown amount of non-plastic inclusions (%) 20% dominant: µm (monocrystalline )maximum: 2300 µm (carbonate rock fragment) orientation not visible 1 N light yellowish brown + N brownish yellow isotropy average thickness 1500µm boundary diffuse composition non-plastic inclusions mineral fragments monocrystalline AB low sphericity, angulat, normal extinction µm polycrystalline R high sphericity, well rounded;low sphericity, subrounded µm potassium R muscovite R carbonate rock fragments INT low sphericity, well rounded, subrounded µm
2 Archeometriai Műhely 2007/2., Supplement for Gherdán et al. 2 75/b 1 N brown + N brown amount of non-plastic inclusions (%) 30% dominant: µm (monocrystalline and polycrystalline, carbonate )maximum: 2500 µm (carbonate rock fragment) orientation elongated pores parallel to surface (pores also around bigger carbonate ) 1 N redish brown + N redish brown isotropy average thickness 2000 µm boundary diffuse composition non-plastic inclusions mineral fragments monocrystalline INT low sphericity, angular; normal extinction µm polycrystalline INT high sphericity, well rounded (bigger ones);low sphericity, µm subrounded (smaller ones) potassium R carbonate rock fragments AB low sphericity, well rounded µm
3 Archeometriai Műhely 2007/2., Supplement for Gherdán et al. 3 75/04 1 N brown + N yellowish brown amount of non-plastic inclusions (%) 10% dominant: µm (monocrystalline )maximum: 1300 µm (grog) orientation non-plastic inclusions parallel elongated pores 1 N - + N - isotropy - average thickness - boundary - composition - monocrystalline R/INT low sphericity, angular, normal extinction µm polycrystalline R low sphericity, subrounded µm carbonate rock R low sphericity, well rounded(also present in grog fragments) µm fragments grog INT isometric or elongated fragments with sharp edges, composition µm and texture is
4 Archeometriai Műhely 2007/2., Supplement for Gherdán et al. 4 75/02 1 N brownish yellow + N yellowish brown amount of non-plastic inclusions 10% dominant: µm (monocrystalline )maximum: 1500 µm (grog, carbonate rock fragment) orientation elongated pores parallel to surface 1 N - + N - isotropy - average thickness - boundary - composition - non-plastic inclusions mineral fragments monocrystalline R/INT low sphericity, angular, low sphericity rounded, low sphericity, µm subrounded; normal extinction R low sphericity, high sphericity rounded, subrounded µm polycrystalline potassium R carbonate rock ACC low sphericity, subrounded 1500 µm fragment others grog INT isometric or elongated fragments with sharp boundaries, composition, sometimes contain low sphericity, well rounded carbonate µm
5 Archeometriai Műhely 2007/2., Supplement for Gherdán et al. 5 80/a 1 N brownish yellow + N yellowish brown amount of non-plastic inclusions (%) 20% dominant: µm (grog)maximum: 3000 µm (grog) orientation inhomogenous matrix with flow structures 1 N - + N - isotropy - average thickness - boundary - composition - non-plastic inclusions mineral fragments monocrystalline R low sphericity, angular; normal extinction µm polycrystalline potassium R muscovite accessories carbonate rock fragments others grog AB isometric or elongated, with sharp boundaries; composition is R low sphericity, angular; low sphericity, subrounded µm ACC ACC R low sphericity, well rounded µm µm
6 Archeometriai Műhely 2007/2., Supplement for Gherdán et al. 6 75/c 1 N brownish yellow + N yellowish brown amount of non-plastic inclusions (%) 10% dominant: µm (grog)maximum: 1500 µm (grog) orientation inhomogenous matrix with flow structures 1 N - + N - isotropy - average thickness - boundary - composition - non-plastic inclusions mineral fragments monocrystalline R low sphericity, angular; normal extinction µm polycrystalline R low sphericity, subrounded µm carbonate rock R low sphericity, well rounded µm fragment others grog AB elongated fragments with sharp boundaries, composition is similar to bulk µm
7 Archeometriai Műhely 2007/2., Supplement for Gherdán et al. 7 75/a 1 N brownish yellow + N yellowish brown amount of non-plastic inclusions (%) 10% dominant: µm (grog)maximum: 1250 µm (grog) orientation it is well visible macroscopically but not in the thin section inhomogenous matrix with flow structures 1 N - + N - isotropy - average thickness - boundary - composition - non-plastic inclusions mineral fragments monocrystalline R low sphericity, angular; normal extinction µm polycrystalline plagioclase muscovite accessories carbonate rock fragments others grog A isometric or elongated fragments with sharp boundaries, composition is, sometimes containing low sphericity, well rounded carbonate ACC low sphericity, subrounded µm ACC ACC ACC R low sphericity, well rounded(also in grog fragments) µm µm
8 Archeometriai Műhely 2007/2., Supplement for Gherdán et al. 8 xx/1/3/a 1 N yellowish brown + N yellowish brown amount of non-plastic inclusions (%) 5% dominant: µm (monocrystalline )maximum: 1750 µm (carbonate shell) 1 N light yellowish brown + N light yellowish brown isotropy average thickness 2000 µm boundary diffuse composition non-plastic inclusions mineral fragments monocrystalline INT low sphericity, angular; normal extinction µm polycrystalline R high sphericity, subrounded µm carbonate rock R low sphericity, well rounded µm fragments others carbonate shell R argillaceous fragments, probably grog R isometric or elongated, with sharp boundaries; is black, isotropy is strong µm
9 Archeometriai Műhely 2007/2., Supplement for Gherdán et al. 9 75/05 1 N brown + N dark brown strong amount of non-plastic inclusions (%) 20% dominant: µm (mineral fragments)maximum: 1000 µm (grog) 1 N - + N - isotropy - average thickness - boundary - composition - non-plastic inclusions mineral fragments monocrystalline AB low sphericity, angular; normal extinction µm polycrystalline R low sphericity, subrounded µm carbonate rock ACC high sphericity, well rounded µm fragment others grog INT isometric or elongated, with sharp boundaries, composition is µm
10 Archeometriai Műhely 2007/2., Supplement for Gherdán et al /01 1 N yellowish brown + N dark yellowish brown amount of non-plastic inclusions (%) 20% dominant: µm (mineral fragments)maximum: 2500 µm (grog) orientation parallel elongated pores it is well visible 1 N - macroscopically but not in the thin + N - section isotropy - average thickness - boundary - composition - non-plastic inclusions mineral fragments monocrystalline AB low sphericity, angular, low sphericity, subrounded; normal µm extinction polycrystalline R low sphericity, subrounded µm carbonate rock ACC low sphericity, well rounded µm fragments others grog AB elongated or isometric with sharp boundaries, composition is µm
11 Archeometriai Műhely 2007/2., Supplement for Gherdán et al /1a/c 1 N yellowish brown + N yellowish brown amount of non-plastic inclusions (%) 20% dominant: µm; µm (mineral fragments; grog)maximum: 3000 µm (grog) it is well visible 1 N - macroscopically but not in the thin + N - section isotropy - average thickness - boundary - composition - non-plastic inclusions mineral fragments monocrystalline polycrystalline potassium plagioclase muscovite accessories carbonate rock INT low sphericity, angular; normal extinction µm ACC low sphericity, subrounded µm ACC ACC ACC ACC ACC low sphericity, well rounded µm fragments others grog AB elongated with sharp boundaries, composition is ; some grains contain other argillaceous fragments µm
12 Archeometriai Műhely 2007/2., Supplement for Gherdán et al. 12 xx/b 1 N brown + N dark brown amount of non-plastic inclusions (%) 15% dominant: µm; µm (mineral fragments; grog)maximum: 3000 µm (grog) 1 N redish brown + N redish brown isotropy average thickness 700 µm boundary sharp composition non-plastic inclusions mineral fragments monocrystalline AB low spheriicty, angular; normal extinction µm polycrystalline R low sphericity, subrounded, rounded µm carbonate rock ACC low sphericity, subrounded 800 µm fragments others grog AB elongated or isometric fragments, composition is, sometimes contain other argillaceous fragments µm
13 Archeometriai Műhely 2007/2., Supplement for Gherdán et al. 13 xx1/3/d 1 N dark brown + N black strong amount of non-plastic inclusions (%) 20% dominant: µm; µm (mineral fragments; grog)maximum: 2500 µm (grog) orientation elongated pores parallel to surface 1 N brown + N redish brown isotropy average thickness 1500µm boundary sharp composition non-plastic inclusions mineral fragments monocrystalline AB low sphericity, angular; (some bigger fragments are high µm sphericity, subangular, subrounded) normal extinction polycrystalline R low sphericity, subrounded µm carbonate rock INT low sphericity (some high sphericity), rounded µm fragment others carbonate shell ACC 1000 µm grog AB isometric or elongated fragments, sometimes with an, µm composition is clay pellet R destorted shape, or well rounded, composition is
14 Archeometriai Műhely 2007/2., Supplement for Gherdán et al. 14 xx4f 1 N brown + N yellowish brown amount of non-plastic inclusions (%) 15 % dominant: µm (mineral fragments)maximum: 4000 µm (grog) 1 N - + N - isotropy - average thickness - boundary - composition - non-plastic inclusions mineral fragments monocrystalline INT low sphericity, angular; normal extinction µm polycrystalline ACC low sphericity, subangular µm carbonate rock R low sphericity, subrounded, well rounded µm fragment others grog INT elongated fragments with sharp boundaries, composition is similar to bulk µm
15 Archeometriai Műhely 2007/2., Supplement for Gherdán et al. 15 xx/1/3/c 1 N dark brown + N black strong amount of non-plastic inclusions (%) 20% dominant: µm; µm (mineral fragments; grog)maximum: 2500 µm (grog) orientation elongated pores parallel to surface 1 N light brown, reddish brown + N brown, reddish brown isotropy average thickness 1000 µm boundary sharp composition non-plastic inclusions mineral fragments monocrystalline A low sphericity, angular, normal extinction µm polycrystalline ACC high sphericity, subrounded 300 µm carbonate rock INT low sphericity, well rounded µm fragment others grog AB isometric or elongated fragments with sharp boundaries, µm composition is, contain other argillaceous fragments sometimes 75/06 1 N dark brown + N dark brown, black
16 Archeometriai Műhely 2007/2., Supplement for Gherdán et al. 16 strong amount of non-plastic inclusions (%) 15% dominant: µm; µm (mineral fragments; grog)maximum: 2500 µm (grog) 1 N - + N - isotropy - average thickness - boundary - composition - non-plastic inclusions mineral fragments monocrystalline AB low sphericity, angular, normal extinction µm polycrystalline ACC low sphericity, subrounded 500 µm carbonate rock R low sphericity, subrounded µm fragment others grog AB isometric or elongated, composition is µm
17 Archeometriai Műhely 2007/2., Supplement for Gherdán et al /03 1 N brown + N dark brown amount of non-plastic inclusions (%) 15% dominant: µm (mineral fragments)maximum: 1300 µm (grog) 1 N - + N - isotropy - average thickness - boundary - composition - non-plastic inclusions mineral fragments monocrystalline AB low sphericity, angular; normal extinction µm polycrystalline R low sphericity, subrounded, subangular µm carbonate rock R low sphericity, high sphericity,well rounded µm fragment others grog INT isometrical or elongated, with sharp boundaries, composition is µm
18 Archeometriai Műhely 2007/2., Supplement for Gherdán et al. 18 xx/c 1 N dark brown + N dark brown strong amount of non-plastic inclusions (%) 15% dominant: µm (mineral fragments)maximum: 1000 µm (grog) 1 N - + N - isotropy - average thickness - boundary - composition - non-plastic inclusions mineral fragments monocrystalline AB low sphericity, angular µm polycrystalline R low sphericity, subangular µm others grog INT isometric or elongated, with sharp boundaries, composition is µm
19 Archeometriai Műhely 2007/2., Supplement for Gherdán et al. 19 xx/e 1 N brown + N dark brown, black strong amount of non-plastic inclusions (%) 20% dominant: µm (mineral fragments)maximum: 1500 µm (grog) 1 N redish brown + N brownish red isotropy average thickness 2000 µm boundary sharp composition, seems to be finer grained, does not contain grog non-plastic inclusions mineral fragments monocrystalline AB low sphericity, angular; normal extinction µm polycrystalline R low sphericity, subangular, high sphericity, well rounded µm others grog INT isometric or elongated, composition is, with sharp boundaries µm
20 Archeometriai Műhely 2007/2., Supplement for Gherdán et al. 20 xx/d 1 N brown + N dark brown, black strong amount of non-plastic inclusions (%) 20% dominant: µm; µm (mineral fragments; grog)maximum: 4000 µm 1 N greyish brown + N redish greyish brown isotropy average thickness 2500 µm boundary diffuse composition non-plastic inclusions mineral fragments monocrystalline AB low sphericity, angular; normal extinction µm polycrístalline R low sphericity, subangular µm others grog AB elongated or isometrical fragments, composition is with less non-plastic inclusions µm
21 Archeometriai Műhely 2007/2., Supplement for Gherdán et al. 21 xx/1/3/b 1 N brown + N dark brown amount of non-plastic inclusions (%) 25% dominant: ; µm (mineral fragments; grog)maximum: 4000 µm (grog) 1 N light brown + N dark yellowish brown isotropy average thickness 1500 µm boundary sharp composition non-plastic inclusions mineral fragments monocrystalline AB low sphericity, angular; normal extinction µm polycrystalline R low sphericity, subrounded; high sphericity, subrounded µm others grog AB elongated fragments, with sharp boundaries, composition is similar to bulk µm
22 Archeometriai Műhely 2007/2., Supplement for Gherdán et al. 22 xx2b 1 N brown + N dark yellowish brown amount of non-plastic inclusions (%) 15% dominant: µm (mineral fragments)maximum: 1300 µm (grog) 1 N yellowish brown/dark yellowish brown + N dark yellowish brown isotropy / average thickness 1500 µm boundary sharp composition non-plastic inclusions mineral fragments monocrystalline AB low sphericity, angular; normal extinction µm carbonate rock ACC low sphericity, well rounded µm fragments others grog INT elongated or isometrical fragments, with sharp boundaries; composition is µm
23 Archeometriai Műhely 2007/2., Supplement for Gherdán et al /1a/a 1 N yellowish brown + N dark yellowish brown amount of non-plastic inclusions (%) 25% dominant: µm; µm (mineral fragments; grog)maximum:2500 µm (grog) 1 N greyish yellowish brown + N yellowish brown isotropy average thickness 1500 µm boundary diffuse composition non-plastic inclusions mineral fragments monocrystalline AB low sphericity, angular, normal extinction µm polycrystalline R low sphericity, subangular µm s s R others grog AB elongated or isometrical fragments with sharp boundaries, composition is, sometime containing other argillaceous fragments as well µm
24 Archeometriai Műhely 2007/2., Supplement for Gherdán et al /1a/b 1 N brown + N yellowish brown amount of non-plastic inclusions (%) 10% dominant: µm (mineral fragments)maximum:1300 µm (grog) 1 N yellowish brown + N dark yellowish brown isotropy average thickness 2000 µm boundary diffuse composition non-plastic inclusions mineral fragments monocrystalline AB low sphericity, angular; normal extinction µm polycrystalline R low sphericity, subrounded, subangular µm others grog INT isometrical or elongated fragments with sharp boundaries, composition is µm
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